Update to biogenic silica dissolution rates in WOMBATmid#110
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…ling base Bsi dissolution rates Removed the 2 exponent on Bsi dissolution due to undersaturation to align with thermodynamics Updated the docs.
pearseb
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Apr 30, 2026
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| _where_ <br> | ||
| - $T_{K}$ is the in situ temperature of seawater ([`zval`, [ºK]]) <br> | ||
| - $T_{K}$ is the in situ temperature of seawater ([`zval`, [ºK]) <br> |
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| - $T_{K}$ is the in situ temperature of seawater ([`zval`, [ºK]) <br> | |
| - $T_{K}$ is the in situ temperature of seawater (`zval`, [ºK]) <br> |
pearseb
commented
Apr 30, 2026
| @@ -1446,7 +1446,7 @@ _where_ <br> | |||
| - $T_{K}$ is the in situ temperature of seawater ([`zval`, [ºK]]) <br> | |||
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| - $T_{K}$ is the in situ temperature of seawater ([`zval`, [ºK]]) <br> | |
| - $T_{K}$ is the in situ temperature of seawater (`zval`, [ºK]) <br> |
pearseb
commented
Apr 30, 2026
| @@ -1446,7 +1446,7 @@ _where_ <br> | |||
| - $T_{K}$ is the in situ temperature of seawater ([`zval`, [ºK]]) <br> | |||
| - $P$ is the in situ pressure [`zm(i,j,k) * 1.0e4`, [Pa]] <br> | |||
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| - $P$ is the in situ pressure [`zm(i,j,k) * 1.0e4`, [Pa]] <br> | |
| - $P$ is the in situ pressure (`zm(i,j,k) * 1.0e4`, [Pa]) <br> |
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@dougiesquire - no need to attend to this for some weeks. Leave it at the bottom of your to-do list. |
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Introduced
bsi_alphaas a runtime field_table parameter for controlling base Bsi dissolution ratesRemoved the 2 exponent on Bsi dissolution due to undersaturation to align with thermodynamics.
Updated the docs.
These updates come from conversations with Jim Greenwood at CSIRO.